Temporal range: Middle Cambrian–Recent (total group)
Loricifera (from Latin, lorica, corselet (armour) + ferre, to bear) is a phylum of very small to microscopic marine cycloneuralian sediment-dwelling animals with 37 described species, in nine genera. Aside from these described species, there are approximately 100 more that have been collected and not yet described. Their sizes range from 100 µm to ca. 1 mm. They are characterised by a protective outer case called a lorica and their habitat, which is in the spaces between marine gravel to which they attach themselves. The phylum was discovered in 1983 by Roberto Ramos, in Roscoff, France. They are among the most recently discovered groups of Metazoans. They attach themselves quite firmly to the substrate, and hence remained undiscovered for so long. The first specimen was collected in the 1970s, and later described in 1983. They are found at all depths, in different sediment types, and in all latitudes.
The animals have a head, mouth and digestive system as well as a lorica. The armor-like lorica consists of a protective external shell or case of encircling plicae. There is no circulatory system and no endocrine system. Many of the larvae are acoelomate, with some adults being pseudocoelomate, and some remaining acoelomate. Development is generally direct, though there are so-called Higgins larvae, which differ from adults in several respects. The animals have two sexes as adults. Very complex and plastic life cycles of pliciloricids include also paedogenetic stages with different forms of parthenogenetic reproduction. Fossils have been dated to the late Cambrian.
Morphological studies have traditionally placed the phylum in the vinctiplicata with the Priapulida; this plus the Kinorhyncha constitutes the taxon Scalidophora. The three phyla share four characters in common — chitinous cuticle, rings of scalids on the introvert, flosculi, and two rings of introvert retracts. However, mounting molecular evidence indicates a closer relationship with the Panarthropoda.
The loriciferans are believed to be miniaturized descendants of a larger organism perhaps resembling the Cambrian fossil Sirilorica. However, the fossil record of the microscopic non-mineralized group is (perhaps unsurprisingly) scarce, so it is difficult to trace out the phylum's evolutionary history in any detail. The 2017 discovery of Cambrian-era Eolorica deadwoodensis may shed some light on the group's history.
In anoxic environment
Three species of Loricifera have been found in the sediments at the bottom of the L'Atalante basin in Mediterranean Sea, more than 3,000 meters down, the first multicellular organisms known to spend their entire lives in an oxygen-free environment. They are able to do this because their mitochondria act like hydrogenosomes, allowing them to respire anaerobically.
The newly reported animals complete their life cycle in the total absence of light and oxygen, and they are less than a millimetre in size. They were collected from a deep basin at the bottom of the Mediterranean Sea, where they inhabit a nearly salt-saturated brine that, because of its density (> 1.2 g/cm3), does not mix with the waters above. As a consequence, this environment is completely anoxic and, due to the activity of sulfate reducers, contains sulphide at a concentration of 2.9 mM. Despite such harsh conditions, this anoxic and sulphidic environment is teeming with microbial life, both chemosynthetic prokaryotes that are primary producers, and a broad diversity of eukaryotic heterotrophs at the next trophic level.
- Nanaloricidae Kristensen, 1983
- Pliciloricidae Higgins & Kristensen, 1986
- Urnaloricidae Heiner & Møbjerg Kristensen, 2009
- Urnaloricus Heiner & Møbjerg Kristensen, 2009
- Extinct taxa (unclassified)
- †Eolorica Harvey & Butterfield, 2017
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|Wikispecies has information related to Loricifera|
- Bernhard, Joan M.; Morrison, Colin R.; Pape, Ellen; Beaudoin, David J.; Todaro, M. Antonio; Pachiadaki, Maria G.; Kormas, Konstantinos Ar.; Edgcomb, Virginia P. (2015). "Metazoans of redoxcline sediments in Mediterranean deep-sea hypersaline anoxic basins". BMC Biology. 13: 105. doi:10.1186/s12915-015-0213-6. PMC 4676161. PMID 26652623.
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